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Information Journal Paper

Title

STUDY OF GOLMAKAN'S PLANT MACROFOSSILES, NORTH EAST OF IRAN

Pages

  98-107

Abstract

 Binalud Mountain is geographically the continuation of Alborz Mountain but because of some facies similarities and the effects of folding, it is considered to be the transition zone between Central IRAN and Alborz. In this study, eight PLANT MACROFOSSIL species are identified from Shemshak Formation in Golmakan, BINALUD. They are Coniopteris hymenophylloides, Klukia westi, Sphenobaiera longifolia, Sphenobaiera cf. pulchella, Czekanowskia rigida, Nilssonia macrophylla, Nilssonia acuminata and Nilssonia feriziensis. According to their stratigraphical distribution, Late Liassic - Early Dogger age canbe inferreded for this assemblage.

Cites

References

Cite

APA: Copy

VAEZ JAVADI, F., & POUR LATIFI, A.. (2004). STUDY OF GOLMAKAN'S PLANT MACROFOSSILES, NORTH EAST OF IRAN. GEOSCIENCES, 11(51-52), 98-107. SID. https://sid.ir/paper/31956/en

Vancouver: Copy

VAEZ JAVADI F., POUR LATIFI A.. STUDY OF GOLMAKAN'S PLANT MACROFOSSILES, NORTH EAST OF IRAN. GEOSCIENCES[Internet]. 2004;11(51-52):98-107. Available from: https://sid.ir/paper/31956/en

IEEE: Copy

F. VAEZ JAVADI, and A. POUR LATIFI, “STUDY OF GOLMAKAN'S PLANT MACROFOSSILES, NORTH EAST OF IRAN,” GEOSCIENCES, vol. 11, no. 51-52, pp. 98–107, 2004, [Online]. Available: https://sid.ir/paper/31956/en

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